Low-degree melt metasomatic origin of heavy Fe isotope enrichment in the MORB mantle-Reference-Cited by-同舟云学术

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Low-degree melt metasomatic origin of heavy Fe isotope enrichment in the MORB mantle

Published:2023-01 Issue: Volume:601 Page:117892
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Guo Pengyuan,Niu Yaoling^ORCID,Chen Shuo,Duan Meng,Sun Pu,Chen Yanhong^ORCID,Gong Hongmei,Wang Xiaohong

Funder

National Natural Science Foundation of China

National Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers

Higher Education Discipline Innovation Project

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference58 articles.

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2. Contrasting volcanictectonic processes during the past 2 Ma on the Mid-Atlantic Ridge: submersible mapping, petrological and magnetic results at lat. 34°52′N and 33°55′N;Bideau;Mar. Geophys. Res.,1998

3. Ferric iron in peridotites and mantle oxidation states;Canil;Earth Planet. Sci. Lett.,1994

4. Iron isotope fractionation during mid-ocean ridge basalt (MORB) evolution: evidence from lavas on the East Pacific Rise at 10°30′ N and its implications;Chen;Geochim. Cosmochim. Acta,2019

5. Simple and cost-effective methods for precise analysis of trace element abundances in geological materials with ICP-MS;Chen;Sci. Bull.,2017

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